Rock Identifier
Granite (Phaneritic Plutonic Felsic Rock) — igneous
igneous

Granite

Phaneritic Plutonic Felsic Rock

Hardness: 6-7 on Mohs scale. Color: Salt-and-pepper look with pink/white/grey crystals. Luster: Vitreous to dull. Structure: Coarse-grained phaneritic. Composition: Primarily quartz, alkali feldspar, and plagioclase with minor mica/amphibole.

Hardness
6-7 on Mohs scale
Color
Salt-and-pepper look with pink/white/grey crystals
Luster
Vitreous to dull
Identified More igneous
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Physical properties

Hardness: 6-7 on Mohs scale. Color: Salt-and-pepper look with pink/white/grey crystals. Luster: Vitreous to dull. Structure: Coarse-grained phaneritic. Composition: Primarily quartz, alkali feldspar, and plagioclase with minor mica/amphibole.

Formation & geological history

Formed from the slow crystallization of silica-rich magma beneath the Earth's surface (intrusive). They can be hundreds of millions to billions of years old, often found in the cores of mountain ranges.

Uses & applications

Extensively used in construction for countertops, floor tiles, paving stones, curbing, monuments, and as crushed stone for road aggregate.

Geological facts

Granite makes up much of the Earth's continental crust. Mount Rushmore is carved into a granite batholith. It is one of the hardest natural stones commonly available.

Field identification & locations

Identify by its interlocking visible crystals. Look for flecks of clear/white quartz and pink or white rectangular feldspar crystals. It is found in continental shields and mountain belts globally.